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Early cretaceous subduction-related adakite
Early cretaceous subduction-related adakite

... belt. To explore this issue, we present SHRIMP U–Pb zircon data and geochemical and Sr–Nd–Pb–Hf isotopic data for the Mamen andesites from the southern margin of the Gangdese Belt. The Mamen andesites, emplaced at 136.5 Ma, are sodic (Na2O/K2O = 1.2–2.3) and have geochemical characteristics typical ...
6th Grade Earth Science
6th Grade Earth Science

... Rocks • _____ - a solid, natural material made up of rock one or more minerals Rock cycle • ___________ - as time passes, rock break down, and the minerals in them are recycled – pattern of change • The rock cycle takes place over millions ________ of years. • There are three types of rocks: ______ ...
Slide 1
Slide 1

... 2) Continental collision takes place because buoyancy forces do not allow large amount of continental subduction 3) During continental collision tectonics deformation is not anymore localized along the plate margin (accretionary wedge), but affects a large area in the upper plate and propagate crato ...
Benchmark (IMEDL 2004)
Benchmark (IMEDL 2004)

... What is the effect of preexisting weakness (suture zone, orogeny) in the lithosphere? What is the role of the lower crust if it is partly composed of gabbros? ...
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... B wet areas with low temperatures C moist areas with warm temperatures D dry areas with low temperatures Which of the following lists the correct sequence in the formation of a sedimentary rock? A B C D ...
Practice Quiz 2
Practice Quiz 2

... B Chemical sediment is formed by processes such as evaporation and precipitation, whereas biochemical sediment is formed by processes driven by living marine organisms C Chemical sediment is formed by the reworking of animal shells, whereas biochemical sediment is formed in caves by water dripping f ...
PACHUCA PROJECT Municipality of Atotonilco El Grande, Hidalgo
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The Penokean orogeny in the Lake Superior region
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LOCAL AND REGIONAL GEOLOGY
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... is by far the most important lithology of this massif. Towards the north coast coarse-grained arenite becomes more important, and the slates develop into mica schists intruded by occasional masses of gabbro. At the eastern end of the Dili massif, near Manatuto the rocks include hornblende gneiss and ...
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... Earthquake - a vibration produced by the rapid release of stored energy. The focus is the source of the quake, typically on a fault or plane of slippage in the Earth's crust The epicenter is the point on the Earth's surface immediately above the focus, determined from the seismic waves generated by ...
the petrology of iceland some general remarks
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... tcpographic features as f.i. Eldgja. The length of both individual fissures and rift swarms varies greatly. Their age is most probably varyable as well; which means that they are in different stages of evolution. The main rift swarms of the present rift zones are shown schematically in Fig. 6. It wa ...
Abstract  - Dalhousie University
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... strongly deformed, is largely derived from contiguous Indian middle crust. Particle tracking indicates little or no mixing of diverse crustal elements in the exhumed region, so that units exposed at the surface could appear to retain a coherent "stratigraphy". However, in the model, this material ha ...
Geological History
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... Early Paleozoic marked by 6 different landmasses that will come together to form Pangea at the end of the Paleozoic. Paleozoic characterized by major mountain building events such as the Appalachians, the Urals, and the Caledonides. Ancestral North America collided with Africa to produce the origina ...
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Magma Type and Plate Margins

... Large blocks close to the vent ...
Activity Source: Adapted from the USGS Learning Web Lesson
Activity Source: Adapted from the USGS Learning Web Lesson

... One of the most frightening and destructive phenomena of nature is a severe earthquake and its terrible aftereffects. An earthquake is a sudden movement of the Earth, caused by the abrupt release of strain that has accumulated over a long time. For hundreds of millions of years, the forces of plate ...
Geology - Lake Champlain Maritime Museum
Geology - Lake Champlain Maritime Museum

... Americans in this region had been picking up certain fragments of rock—mainly quartzite and chert—to fashion them into projectile points and other tools with which to hunt, fish, work hides, and perform other tasks necessary to survival. We see the results of weathering everywhere we look. Rock bodi ...
Plate Tectonics
Plate Tectonics

... floor spreading in 1962. • Sea Floor Spreading Theory- idea that the seafloor moves and carries the continents with it. • Caused by divergent boundaries moving apart and allowing the liquid like asthenosphere to move upward and cool creating new oceanic crust. ...
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Algoman orogeny



The Algoman orogeny, known as the Kenoran orogeny in Canada, was an episode of mountain-building (orogeny) during the Late Archean Eon that involved repeated episodes of continental collisions, compressions and subductions. The Superior province and the Minnesota River Valley terrane collided about 2,700 to 2,500 million years ago. The collision folded the Earth's crust and produced enough heat and pressure to metamorphose the rock. Blocks were added to the Superior province along a 1,200 km (750 mi) boundary that stretches from present-day eastern South Dakota into the Lake Huron area. The Algoman orogeny brought the Archaen Eon to a close, about 2,500 million years ago; it lasted less than 100 million years and marks a major change in the development of the earth’s crust.The Canadian shield contains belts of metavolcanic and metasedimentary rocks formed by the action of metamorphism on volcanic and sedimentary rock. The areas between individual belts consist of granites or granitic gneisses that form fault zones. These two types of belts can be seen in the Wabigoon, Quetico and Wawa subprovinces; the Wabigoon and Wawa are of volcanic origin and the Quetico is of sedimentary origin. These three subprovinces lie linearly in southwestern- to northeastern-oriented belts about 140 km (90 mi) wide on the southern portion of the Superior Province.The Slave province and portions of the Nain province were also affected. Between about 2,000 and 1,700 million years ago these combined with the Sask and Wyoming cratons to form the first supercontinent, the Kenorland supercontinent.
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